以超微技术手段研究细粒碳酸盐岩的结构,可探讨其多种原因,成岩次生变化和孔隙类型,并对其储集性能进行评价。
Studying fine-grained carbonate rocks by ultra-technique can inquire into its various origin, secondary change in diagenesis and type of pores and evaluate its reservior properties.
以超微技术手段研究细粒碳酸盐岩的结构,可探讨其多种原因,成岩次生变化和孔隙类型,并对其储集性能进行评价。
Studying fine-grained carbonate rocks by ultra-technique can inquire into its various origin, secondary change in diagenesis and type of pores and evaluate its reservior properties.
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